Wave Diffraction from A Vertical Cylinder with Two Uniform Columns and Porous Outer Wall
Bibliographic record
Abstract
［1］Chwang, A.T.,1983. A porous-wavemaker theory, J. of Fhuid Mech.,132, 395～406. ［2］Chwang, A.T. and Chan, A. T., 1998. Interaction between porous media and wave motion, Annu. Rev. Mech., 30, 53～84. ［3］Dalrymple, R. A. and Martin, P. A., 1990. Wave diffraction through offshore breakwaters, J. Wtrwy. Harb. and Coast.En grg., ASCE, 116, 727～741. ［4］Dalrymple, R. A., Losada, M. A. and Martin, P. A., 1991. Reflection and transmission from porous structures under oblique wave attack, J. Fluid Mech., 224, 625～644. ［5］Madsen, O. S., 1974. Wave transmission through porous structures, J. Wtrwv. Harb. and Coast. Engrg. Div., ASCE, 102(1), 169～188. ［6］Sollitt, C. K. and Cross, R. H, 1972. Wave transmission through permeable breakwaters, Proceedings of the 13th CoastalEngineering Conference, ASCE, Vancouver, B. C., Canada, 1827～1846. ［7］Twu, S. W. and Lin, D. T., 1990. Wave reflection by a number of thin porous plates fixed in a semi-infinitely long flume,Proceedings of the 22nd Coastal Engineering Conference, ASCE, Delft, The Netherlands, 1046～1059. ［8］YANG, G., 1996. Numerical model of wave effects on perneable vertical barriers above the seabed, MASc thesis, Dept. of Civil Engrg., University of British Columbia, Vancouver, Canada. ［9］YU, X. P., 1995. Diffraction of water waves by porous breakwaters, J. Wtrwy. Port, Coastal and Ocean Engrg., ASCE,121 (6), 275～282. ［10］ZHU, S. and Chwang A. T., 1998. Performance of a caisson-type porous wave absorber, Proc. of Int. Hydrodynamics,Seoul. 2, 913～918. ［11］WU, J. H., WAN, Z. P. and FANG, Y., 1998. Wave trapping near the vertical wall due to a horizontal submerged porous plate, J. of Hydrodynamics, Ser. A, 13 (1), 49～58. (in Chinese)
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How this classification was reachedexpand
Full frame distilled prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.000 | 0.000 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.004 | 0.000 |
Machine scores (provisional)
The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.
Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one teacher head, not a consensus.
How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".